Abstract
The transitions induced by temperature and pressure between the face-centered cubic (fcc) and the body-centered cubic (bcc) phases in the alkaline earth metals—Ca, Sr, and Ba—are analyzed by computing the differences in Gibbs free energy between the two phases in the framework of the nearly-free-electron and harmonic approximations. At the absolute zero of temperature and pressure, the observed fcc in Sr and bcc in Ba were found to have the lower internal energy; in Ca, however, identical analysis led to lower energy in bcc rather than the observed fcc. An fcc-bcc transition characterized by a change in the sign of the difference in free energies in Sr at 0°K was found at a critical pressure Pc10 kbar; at zero pressure, it was found at a critical temperature, Tc150°K. Both these results agree only qualitatively with the observed Pc36 kbar and Tc830°K. Ca and Ba, already bcc at absolute zero, showed no phase transition.